Abstract
The compositions of 32 granitic rocks of the Damara Orogen (red granites, grey granites, Donkerhoek granites, and Salem granites) show that there is a very broad spectrum of granitic and granodioritic rocks that have been intruded during the long lasting magmatic activity in the Central Zone of the Damara Orogen. No compositional grouping can be made according to the type of granite.
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